ZHANG Shaotong, JIA Yonggang, GUO Lei, LIU Xiaolei, WEN Mingzheng, SHAN Hongxian. IN-SITU OBSERVATION OF SEDIMENT DEPOSITION PROCESS IN CHENGDAO SEA AREA OF THE YELLOW RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2016, 36(3): 171-181. DOI: 10.16562/j.cnki.0256-1492.2016.03.017
Citation: ZHANG Shaotong, JIA Yonggang, GUO Lei, LIU Xiaolei, WEN Mingzheng, SHAN Hongxian. IN-SITU OBSERVATION OF SEDIMENT DEPOSITION PROCESS IN CHENGDAO SEA AREA OF THE YELLOW RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2016, 36(3): 171-181. DOI: 10.16562/j.cnki.0256-1492.2016.03.017
shu

IN-SITU OBSERVATION OF SEDIMENT DEPOSITION PROCESS IN CHENGDAO SEA AREA OF THE YELLOW RIVER ESTUARY

  • 1. Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, Ocean University of China, Qingdao 266100;

  • 2. Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266200;

  • 3. Key Laboratory of Marine Environment and Ecology, Ministry of Education, Ocean University of China, Qingdao 266100

More Information
  • Received Date: August 06, 2015
  • Revised Date: March 19, 2016
    Graphical Abstract
    • Abstract
  • The in-situ measured amount of deposits was obtained in the Chengdao sea area off the Yellow River Estuary using a time-series sediment trap. Combined with the synchronous hydrodynamic observation and subsequent laboratorial grain size analysis, we firstly calculated the depositional flux, and subsequently analyzed the source of trapped sediments, then discussed the influence factors of depositional process, and finally evaluated its proportion in the resuspended sediments. The results indicate that the sediment depositional flux in the Chengdao sea area is around 120~280 g·m-2·d-1. The depositional fluxes show a positive correlation with the re-suspended deposits possibly indicating that the deposited sediments maybe mainly come from the re-suspension of bottom sediments. Sediment deposition still occurs even the excess shear stress is greater than zero, and the amount of deposition may be greater than that when excess shear stress is intermittently less than zero. This is inferred as the consequence of the liquefaction properties of silty seabed in the area. About 5% of the resuspended sediments deposit in-situ, and most of them remain in suspension or will be transported elsewhere, which may be the reason of intense erosion of seabed in this area.
    • FullText(HTML)
    • References (28)
  • [1]
    李云海,杨作升,陈坚,等. 东北太平洋中国合同区悬浮颗粒物元素地球化学[J]. 海洋地质与第四纪地质,2008,28(5):45-53.

    [LI Yunhai, YANG Zuosheng, CHEN Jian, et al. Characteristics of the element geochemistry of the suspended matter in the Chinese Contract area, Northeast Pacific Ocean[J]. Marine Geology and Quaternary Geology, 2008, 28(5):45-53.]
    [2]
    高抒.海岸与陆架沉积:动力过程、全球变化影响和地层记录[J]. 第四纪研究,2010, 30(5):856-863.

    [GAO Shu. Coastal and shelf sedimentation in association with dynamic processes, global change impacts, and stratigraphic records:an overview of the scientific problems[J]. Quaternary Sciences, 2010, 30(5):856-863.]
    [3]
    Liu J T, Hung J J, Lin H L, et al. From suspended particles to strata:The fate of terrestrial substances in the Gaoping(Kaoping)submarine canyon[J]. Journal of Marine System, 2009, 76(4):417-432.
    [4]
    洪华生,徐立,郭劳动. 台湾海峡南部、罗源湾和厦门港颗粒垂直通量研究①[J]. 海洋科学,1993(1):47-51.[HONG Huasheng, XU Li, GUO Laodong. Vertical flux study of settling particulate matter in Taiwan Strait, Luoyuan Bay and Xiamen Bay①[J]. Marine Science, 1993

    (1):47-51.]
    [5]
    张岩松,章飞军,郭学武,等. 黄海夏季水域沉降颗粒物垂直通量的研究[J]. 海洋与湖沼,2004,35(3):230-238.

    [ZHANG Yansong, ZHANG Feijun, GUO Xuewu, et al. Vertical flux of the settling particulate matter in the water column of the Yellow Sea in summer[J]. Oceanologia et Limnolgia Sinica, 2004, 35(3):230-238.]
    [6]
    张岩松,章飞军,郭学武,等. 黄海秋季典型站位沉降颗粒物的垂直通量[J]. 地球化学,2005,34(2):123-128.

    [ZHANG Yansong, ZHANG Feijun, GUO Xuewu, et al. Autumn vertical flux of settling particulate matter at three typical stations in the Yellow Sea[J]. Geochimica, 2005, 34(2):123-128.]
    [7]
    杨茜,杨庶,宋娴丽,等. 桑沟湾夏、秋季悬浮颗粒物的沉降通量及再悬浮的影响[J]. 海洋学报, 2014, 36(12):85-90.

    [YANG Qian, YANG Shu, SONG Xianli, et al. Vertical flux and re-suspension of settling particulate matter of Sanggou Bay in summer and autumn[J]. Acta Oceanologica Sinica, 2014, 36(12):85-90.]
    [8]
    刘晓. 黑泥湾海域沉降颗粒物通量及其影响因子研究[D]. 中国科学院海洋研究所博士学位论文, 2012.[LIU Xiao. Study on settling particulate matter flux and impact factors in Harny Bay[D]. Doctoral Dissertation, Institute of Oceanology, Chinese Academy of Sciences, 2012.]
    [9]
    方建勇, 陈坚, 张晓飞, 等. 九龙江河口枯季沉降颗粒物及其地球化学组成研究①[J].沉积学报,2011,29(4):761-766.

    [FANG Jianyong, CHEN Jian, ZHANG Xiaofei, et al. The settling particulate matter and their geochemical compositions in Jiulongjiang Estuary in dry season ①[J]. Acta Sedimentologica Sinica, 2011, 29(4):761-766.]
    [10]
    方建勇,陈坚,刘志飞,等. 2009年春季九龙江口水体沉降颗粒物组分的类型与分布[J]. 应用海洋学学报, 2013,32(3):316-323.

    [FANG Jianyong, CHEN Jian, LIU Zhifei, et al. Types and distribution of the components of settling particulate matter in Jiulongjiang River Estuary in spring of 2009[J]. Journal of Applied Oceanography, 2013,32(3):316-323.]
    [11]
    方建勇,李云海,尹希杰,等. 南极普里兹湾海域夏季表层悬浮颗粒物物质组分研究[J]. 海洋地质与第四纪地质,2015,35(3):175-187.

    [FANG Jianyong, LI Yunhai, YIN Xijie, et al. Composition of summer surficial suspended particles in the Prydz[J]. Marine Geology and Quaternary Geology, 2015, 35(3):175-187.]
    [12]
    郭志刚,杨作升. 东海颗粒碳的垂直转移过程[J]. 海洋与湖沼,1997,28(6):659-664.

    [GUO Zhigang, YANG Zuosheng. Vertical transfer processes for the particulate carbon in the East China Sea[J]. Oceanologia et Limnologia Sinica, 1997, 28(6):659-664.]
    [13]
    詹滨秋, 宋金明, 等.东海沉降悬浮物质的特征研究[J]. 海洋科学集刊, 1993, 34(0):107-113.

    [ZHAN Binqiu, WU Yulin, et al. Study on the characteristics of the sinking matter in the East China Sea[J]. Studia Marina Sinica, 1993, 34(0):107-113.]
    [14]
    李文宝, 王汝建, 陈建芳,等. 南海表层沉积物与水柱中沉降颗粒物对比研究及其古环境再造意义[J]. 海洋地质与第四纪地质,2008,28(4):73-83.

    [LI Wenbao, WANG Rujian, CHEN Jianfang, et al. Correlation of surface sediments with sinking particulate matters in the South China Sea and implication for reconstructing paleoenvironment[J]. Marine Geology and Quaternary Geology, 2008, 28(4):73-83.]
    [15]
    王爱军, 叶翔, 陈坚,等. 沉积物捕获器在海岸与陆架沉积动力研究中的应用:以罗源湾和台湾海峡为例[J]. 海洋学报,2015,37(1):125-136.

    [WANG Aijun, YE Xiang, CHEN Jian, et al. Applications of sediment trap in sediment dynamics in coast and shelf sea:A case study of Luoyuan Bay and Taiwan Strait[J]. Acta Oceanologica Sinica, 2015,37(1):125-136.]
    [16]
    Keller G H, Zhen J, Yang Z S, et al. Mass physical properties of Huanghe delta and Southern Bohai Sea near-surface deposits, China[J]. Marine Georesources and Geotechnology, 1990, 9(3):207-225.
    [17]
    孙永福,董立峰, 蒲高军,等. 风暴潮作用下黄河水下三角洲斜坡稳定性研究[J]. 工程地质学报,2006,14(5):582-587.

    [SUN Yongfu, DONG Lifeng, PU Gaojun, et al. Stability analysis of slope in the subaqueous delta of the Yellow River under storm wave loading[J]. Journal of Engineering Geology, 2006, 14(5), 582-587.]
    [18]
    Krumbein W C. Size frequency distributions of sediments[J]. Journal of Sedimentary Petrology,1934, 4(2):65-77.
    [19]
    Shepard. Nomenclature Based on Sand-silt-clay Ratios[J]. Journal of Sedimentary Petrology, 1954, 24(3):151-158.
    [20]
    蔡立胜, 方建光,董双林. 桑沟湾养殖海区沉积物-海水界面氮、磷营养盐的通量[J]. 海洋水产研究,2004,25(4):57-64.

    [CAI Lisheng, FANG Jianguang, DONG Shuanglin. Preliminary studies on nitrogen and phosphorus fluxes between seawater and sediment in Sungo Bay[J]. Marine Fisheries Research, 2004, 25(4):57-64.]
    [21]
    倪建宇,张美,刘小涯,等.秋季黄海和东海海域沉降颗粒物及其地球化学组成[J]. 海洋学报,2006,28(1):158-162.

    [NI Jianyu, ZHANG Mei, LIU Xiaoya, et al. Sinking particles and their geochemical compositions in the Huanghai and East China Seas in autumn[J]. Acta Oceanologica Sinica, 2006, 28(1):158-162.]
    [22]
    Szmytkiewicz A, Zalewska T. Sediment deposition and accumulation rates determined by sediment trap and 210Pb isotope methods in the Outer Puck Bay (Baltic Sea)[J]. Oceanologia, 2014, 56(1):85-106.
    [23]
    Jhmlich S, Lund-Hansen L Ch, Leipe T. Enhanced settling velocities and vertical transport of particulate matter by aggregation in the benthic boundary layer[J]. Danish Journal of Geography, 2002, 102(1):37-49.
    [24]
    Folk R L, Ward W C. Brazos River bar:a study in the significance of grain size parameters[J]. Journal of Sedimentary Research, 1957, 27(1):3-26.
    [25]
    Dyer K R. Coastal and Estuarine Sediment Dynamics[M]. Chichester:Wiley, 1986:50, 62.
    [26]
    Soulsby R. Dynamics of marine sands[M]. London:Thomas Telford Publication, 1997:104-107.
    [27]
    Jia Jianjun, GAO Shu, XUE Yunchuan. Sediment dynamic processes of the Yuehu inlet system, Shandong Peninsula, China[J]. Estuarine, Coastal and Shelf Science, 2003, 57(5):783-801.
    [28]
    Partheniades, E. Erosion and deposition of cohesive soils[J]. Journal of the Hydraulics Division, American Society of Civil Engineers 91(HY2), 1965, 91(1):105-138.
    • Related Articles

  • Related Articles

    [1]DANG Yao, LIU Surui, WANG Houjie, LU Taian, WU Xiao, BI Naishuang, HU Limin. Distribution, source, and transport of particulate organic carbon in the Yellow River estuary as affected by the water-sediment regulation[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 120-130. DOI: 10.16562/j.cnki.0256-1492.2023012401
    [2]LU Haohao, YANG Yang, TANG Jieping, CHEN Dezhi, XU Yao, WU Ziyin, FAN Haibo, WANG Yaping. Observation of near-bottom transport of suspended sediment in the offshore area of abandoned Yellow River mouth[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 38-48. DOI: 10.16562/j.cnki.0256-1492.2017082801
    [3]LIU Qiang, XIANG Lihui, ZHANG Gang, OUYANG Kai. Distribution pattern of surface sediments around the abandoned Yellow River estuary of North Jiangsu Province and its controlling factors[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 118-126. DOI: 10.16562/j.cnki.0256-1492.2018.01.012
    [4]CHANG Fangqiang, JIA Yonggang. DISASTERS CAUSED BY WAVE-INDUCED SEDIMENT LIQUEFACTION AT THE YELLOW RIVER DELTA,CHINA[J]. Marine Geology & Quaternary Geology, 2011, 31(2): 43-48. DOI: 10.3724/SP.J.1140.2011.02043
    [5]CHEN Youyuan, WANG Junpeng, ZHAO Wenjuan, GAO Leijian, HUANG Tao, YAO Zijuan. THE EFFECT OF CALCIUM CARBONATE ON SEDIMENT AGGREGATION IN THE INTERTIDAL ZONE OF THE YELLOW RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 87-94. DOI: 10.3724/SP.J.1140.2010.04087
    [6]MI BeiBei, YAN Jun, ZHUANG Lihua, LUAN Zhendong. THE TOPOGRAPHICAL AND MORPHOLOGICAL FEATURES OF MODERN YELLOW RIVER MOUTH AREA AND THEIR RELATION TO EROSIONAL/DEPOSITIONAL PROCESSES[J]. Marine Geology & Quaternary Geology, 2010, 30(3): 31-38. DOI: 10.3724/SP.J.1140.2010.03031
    [7]CHEN Youyuan, ZHAO Wenjuan, JIA Yonggang, XU Guohui. THE INFLUENCE OF CLAY AND ORGANIC MATTER ON THE SEDIMENT AGGREGATION IN THE YELLOW RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 31-37. DOI: 10.3724/SP.J.1140.2009.01031
    [8]CHANG Fang-qiang, MENG Xiang-mei, LIU Jing-kun, HE Feng, JIA Yong-gang. STATISTICAL ANALYSIS OF SOIL PROPERTY AT CHENGDAO SEA AREA IN ESTUARY OF YELLOW RIVER[J]. Marine Geology & Quaternary Geology, 2008, 28(6): 35-40. DOI: 10.3724/SP.J.1140.2008.06035
    [9]YANG Xiu-juan, JIA Yong-gang, YUAN Hang, ZHANG Jian, ZHANG Yan-tao, FENG Chun-jian. CASE STUDY ABOUT THE AFFECTED AREA OF BARE PIPELINE ON THE SEABED SOIL IN YELLOW RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2008, 28(6): 27-33. DOI: 10.3724/SP.J.1140.2008.06027
    [10]DONG Hao-gang, Zhang Wei-ming, Jia Yong-gang, Wang Hong-lei. TRANSFORMATION OF GRANULAR COMPOSITION AND MICROSTRUCTURE OF SILT DUE TO CYCLIC LOADING IN YELLOW RIVER ESTUARY,CHINA[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 133-141.

Catalog

    Get Citation
    PDF
    XML
    Article views (2046) PDF downloads (18) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return